Wigand Cathleen, Oczkowski Autumn J, Branoff Benjamin L, Eagle Meagan, Hanson Alana, Martin Rose M, Balogh Stephen, Miller Kenneth M, Huertas Evelyn, Loffredo Joseph, Watson Elizabeth B
Atlantic Coastal Environmental Sciences Division, United States Environmental Protection Agency (US EPA), Narragansett, RI, United States.
Gulf Ecosystem Measurement and Modeling, United States Environmental Protection Agency (US EPA), Gulf Breeze, FL, United States.
Front For Glob Change. 2021 Nov 12;4:1-765896. doi: 10.3389/ffgc.2021.765896.
Tropical mangrove forests have been described as "coastal kidneys," promoting sediment deposition and filtering contaminants, including excess nutrients. Coastal areas throughout the world are experiencing increased human activities, resulting in altered geomorphology, hydrology, and nutrient inputs. To effectively manage and sustain coastal mangroves, it is important to understand nitrogen (N) storage and accumulation in systems where human activities are causing rapid changes in N inputs and cycling. We examined N storage and accumulation rates in recent (1970 - 2016) and historic (1930 - 1970) decades in the context of urbanization in the San Juan Bay Estuary (SJBE, Puerto Rico), using mangrove soil cores that were radiometrically dated. Local anthropogenic stressors can alter N storage rates in peri-urban mangrove systems either directly by increasing N soil fertility or indirectly by altering hydrology (e.g., dredging, filling, and canalization). Nitrogen accumulation rates were greater in recent decades than historic decades at Piñones Forest and Martin Peña East. Martin Peña East was characterized by high urbanization, and Piñones, by the least urbanization in the SJBE. The mangrove forest at Martin Peña East fringed a poorly drained canal and often received raw sewage inputs, with N accumulation rates ranging from 17.7 to 37.9 g y in recent decades. The Piñones Forest was isolated and had low flushing, possibly exacerbated by river damming, with N accumulation rates ranging from 18.6 to 24.2 g y in recent decades. Nearly all (96.3%) of the estuary-wide mangrove N (9.4 Mg ha) was stored in the soils with 7.1 Mg ha sequestered during 1970-2017 (0-18 cm) and 2.3 Mg ha during 1930-1970 (19-28 cm). Estuary-wide mangrove soil N accumulation rates were over twice as great in recent decades (0.18 ± 0.002 Mg hay) than historically (0.08 ± 0.001 Mg hay). Nitrogen accumulation rates in SJBE mangrove soils in recent times were twofold larger than the rate of human-consumed food N that is exported as wastewater (0.08 Mg ha y), suggesting the potential for mangroves to sequester human-derived N. Conservation and effective management of mangrove forests and their surrounding watersheds in the Anthropocene are important for maintaining water quality in coastal communities throughout tropical regions.
热带红树林被称为“海岸之肾”,可促进沉积物沉积并过滤污染物,包括过量营养物质。世界各地的沿海地区人类活动日益增加,导致地貌、水文和养分输入发生变化。为了有效管理和维持沿海红树林,了解人类活动导致氮(N)输入和循环快速变化的系统中的氮储存和积累情况非常重要。我们利用放射性测年的红树林土壤岩芯,研究了圣胡安湾河口(波多黎各圣胡安湾河口)在城市化背景下近几十年(1970 - 2016年)和历史时期(1930 - 1970年)的氮储存和积累速率。当地的人为压力源可直接通过提高土壤氮肥力或间接通过改变水文(如疏浚、填埋和渠化)来改变城郊红树林系统中的氮储存速率。在皮尼翁斯森林和马丁佩尼亚东部,近几十年的氮积累速率高于历史时期。马丁佩尼亚东部城市化程度高,而皮尼翁斯是圣胡安湾河口城市化程度最低的地区。马丁佩尼亚东部的红树林毗邻排水不畅的运河,经常接收未经处理的污水,近几十年来氮积累速率在17.7至37.9克/年之间。皮尼翁斯森林较为孤立,水流冲刷少,可能因筑坝而加剧,近几十年来氮积累速率在18.6至24.2克/年之间。几乎所有(96.3%)河口范围内的红树林氮(9.4 毫克/公顷)都储存在土壤中,其中1970 - 2017年(0 - 18厘米)固存7.1 毫克/公顷,1930 - 1970年(19 - 28厘米)固存2.3 毫克/公顷。近几十年来,河口范围内红树林土壤的氮积累速率(0.18 ± 0.002毫克/公顷·年)是历史时期(0.08 ± 0.001毫克/公顷·年)的两倍多。圣胡安湾河口红树林土壤近期的氮积累速率是作为废水排放的人类消费食物氮速率(0.08毫克/公顷·年)的两倍,这表明红树林具有固存人类来源氮的潜力。在人类世保护和有效管理红树林及其周边流域对于维持热带地区沿海社区的水质至关重要。